Limestone – Đá vôi – CaCO3

[LIST] [*] Limestone – Đá vôi – CaCO3 [/LIST]

Đá vôi (Limestone) và sản phẩm vôi còn được biết đến là những chất có hàm lượng canxi cacbonate hay canxi oxit rất cao lên đến trên 95%, còn lại là hàm lượng magne cacbonat hay oxit chiếm không vượt quá 5%.

Thành phần hóa chất:
CaO 54,60%SiO[SUB]2[/SUB] 0,19%AL[SUB]2[/SUB]O[SUB]3[/SUB] 0,25%Fe[SUB]2[/SUB]O[SUB]3[/SUB] 0,01%MgO 0,55%K[SUB]2[/SUB]O 0,03%Na[SUB]2[/SUB]O 0,01%
Limestone is a sedimentary rock composed largely of the
minerals
calcite and aragonite, which are different crystal forms of calcium carbonate (CaCO[SUB]3[/SUB]). Many limestones are composed from skeletal fragments of marine organisms such as coral or foraminifera.
Limestone makes up about 10% of the total volume of all sedimentary rocks. The solubility of limestone in water and weak acid solutions leads to karst landscapes, in which water erodes the limestone over thousands to millions of years. Most cave systems are through limestone bedrock.
Limestone has numerous uses: as a building material, as aggregate for the base of roads, as white pigment or filler in products such as toothpaste or paints, and as a chemical
feedstock
.
The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778.